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<br />.. <br /> <br />1. 2. 2 <br /> <br />Randomized Seeding Design <br /> <br />~ <br /> <br />A complete change in operational routine was made for the--1~_~8-69 S~~~SO!!, <br />with ran_domi~ed seeding for only one hour of a six-hour intensive data colle~- <br />tion block. Seeding modes included ground gen~_rators at_.Mt. Harr~s, and <br />aircraft seeding, using droppable pyrotechnics or wing flares. Under~ this <br />seeding desIgri-;--the seeding releases were sufficiently short in duration re- <br />lative to the unseeded periods to allow the collection of both seeded and truly <br />unseeded data. Thus, significant results were obtained using this design. <br /> <br />1. 3 Development and Use of Special Equipment and Observing Techniques <br /> <br />It was recognized at the outset that if the project objective were to be accom- <br />plished in the short span of allotted time, high resolution measurements of <br />precipitation rates and vertical profiles of wind, temperature, humidity and <br />stability would be required. Also helpful in isolating seeding effects would <br />be supporting physical measurements such as ice nucleus counts, silver-in- <br />precipitation, and the presence .(or absence) of silver iodide particles acting <br />as snow crystal nuclei. Therefore, a number of special techniques were <br />developed or adapted for use in the experiments. <br /> <br />1. 3. 1 <br /> <br />Precipitation Rate Measurements <br /> <br />" <br /> <br />An optical snow-rate sensor with 2 minute time resolution, capable of opera- <br />ting remotely for a week, was developed and used extensively throughout the <br />project in a dense data collection network. Modified weighing bucket gauges, <br />special Soil Conservation Service snow course water equivalent measurements, <br />and snow pillows were also used as backup data (but with less time resolution). <br /> <br />. <br /> <br />1. 3. 2 <br /> <br />Ice Nucleus Measurements and Inert Tracers <br /> <br />Surface measurements of free air ice nucleus count were made continuously <br />during operational periods at Rabbit Ears Pass, and frequently at additional <br />locations, using an NCAR-Bollay acoustical ice nucleus counter. Phosphor- <br />escent zinc cadmium sulfide was frequently released as a dual tracer simul- <br />taneously with AgI releases during the 1965-66 season, and collected snow <br />samples were melted and analyzed for phosphorescence with the aid of a sen- <br />sitive photo-multiplier device. On a few occasions during the past three <br />seasons, lithium stearate was released as an inert tracer. Air samples <br />were sensed at Rabbit Ears Pass for lithium with a flame photometer, in a <br />cooperative program with the State University of New York at Albany. <br /> <br />1. 3. 3 <br /> <br />Snow Sample Collection and Analysis <br /> <br />.. <br /> <br />During the course of the project two thousand snow samples were collected <br />on 3 ft. x 3 ft. plastic sheets at 5 to 30 minute intervals. These were subse- <br /> <br />. <br /> <br />3 <br /> <br />.........~n. ~ <br />